block uplift
断块差异隆升 differential upwarping of fault-block
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因此，可以通过联合地貌面的级数确定断块隆升的期次，并通过阶地的年代推断断块隆升的起始时间。
Therefore the fault-block uplifting stages can be determined from the steps of unified geomorphic surfaces, and the starting time of uplifting can be deduced from the age of terraces.
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